Application of Landsat‐7 satellite data and a DEM for the quantification of thermokarst‐affected terrain types in the periglacial Lena–Anabar coastal lowland
Extensive parts of Arctic permafrost-dominated lowlands were affected by large-scale permafrost degradation, mainly through Holocene thermokarst activity. The effect of thermokarst is nowadays observed in most periglacial lowlands of the Arctic. Since permafrost degradation is a consequence as well...
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Norwegian Polar Institute
2006
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Online Access: | https://epic.awi.de/id/eprint/57871/ https://epic.awi.de/id/eprint/57871/1/Grosse_2006_PolRes.pdf https://hdl.handle.net/10013/epic.841b7a1b-b37d-4f85-bcc4-17a1249096b7 |
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ftawi:oai:epic.awi.de:57871 2024-09-15T18:02:21+00:00 Application of Landsat‐7 satellite data and a DEM for the quantification of thermokarst‐affected terrain types in the periglacial Lena–Anabar coastal lowland Grosse, Guido Schirrmeister, Lutz Malthus, Timothy J 2006-01-01 application/pdf https://epic.awi.de/id/eprint/57871/ https://epic.awi.de/id/eprint/57871/1/Grosse_2006_PolRes.pdf https://hdl.handle.net/10013/epic.841b7a1b-b37d-4f85-bcc4-17a1249096b7 unknown Norwegian Polar Institute https://epic.awi.de/id/eprint/57871/1/Grosse_2006_PolRes.pdf Grosse, G. orcid:0000-0001-5895-2141 , Schirrmeister, L. orcid:0000-0001-9455-0596 and Malthus, T. J. (2006) Application of Landsat‐7 satellite data and a DEM for the quantification of thermokarst‐affected terrain types in the periglacial Lena–Anabar coastal lowland , Polar Research, 25 (1), pp. 51-67 . doi:10.1111/j.1751-8369.2006.tb00150.x <https://doi.org/10.1111/j.1751-8369.2006.tb00150.x> , hdl:10013/epic.841b7a1b-b37d-4f85-bcc4-17a1249096b7 EPIC3Polar Research, Norwegian Polar Institute, 25(1), pp. 51-67, ISSN: 0800-0395 Article isiRev 2006 ftawi https://doi.org/10.1111/j.1751-8369.2006.tb00150.x 2024-06-24T04:30:12Z Extensive parts of Arctic permafrost-dominated lowlands were affected by large-scale permafrost degradation, mainly through Holocene thermokarst activity. The effect of thermokarst is nowadays observed in most periglacial lowlands of the Arctic. Since permafrost degradation is a consequence as well as a significant factor of global climate change, it is necessary to develop efficient methods for the quantification of its past and current magnitude. We developed a procedure for the quantification of periglacial lowland terrain types with a focus on degradation features and applied it to the Cape Mamontov Klyk area in the western Laptev Sea region. Our terrain classification approach was based on a combination of geospatial datasets, including a supervised maximum likelihood classification applied to Landsat-7 ETM+ data and digital elevation data. Thirteen final terrain surface classes were extracted and subsequently characterized in terms of relevance to thermokarst and degradation of ice-rich deposits. 78 % of the investigated area was estimated to be affected by permafrost degradation. The overall classification accuracy was 79 %. Thermokarst did not develop evenly on the coastal plain, as indicated by the increasingly dense coverage of thermokarst-related areas from south to north. This regionally focused procedure can be extended to other areas to provide the highly detailed periglacial terrain mapping capabilities currently lacking in global-scale permafrost datasets. Article in Journal/Newspaper Climate change Ice laptev Laptev Sea permafrost Polar Research Thermokarst Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Polar Research 25 1 51 67 |
institution |
Open Polar |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
Extensive parts of Arctic permafrost-dominated lowlands were affected by large-scale permafrost degradation, mainly through Holocene thermokarst activity. The effect of thermokarst is nowadays observed in most periglacial lowlands of the Arctic. Since permafrost degradation is a consequence as well as a significant factor of global climate change, it is necessary to develop efficient methods for the quantification of its past and current magnitude. We developed a procedure for the quantification of periglacial lowland terrain types with a focus on degradation features and applied it to the Cape Mamontov Klyk area in the western Laptev Sea region. Our terrain classification approach was based on a combination of geospatial datasets, including a supervised maximum likelihood classification applied to Landsat-7 ETM+ data and digital elevation data. Thirteen final terrain surface classes were extracted and subsequently characterized in terms of relevance to thermokarst and degradation of ice-rich deposits. 78 % of the investigated area was estimated to be affected by permafrost degradation. The overall classification accuracy was 79 %. Thermokarst did not develop evenly on the coastal plain, as indicated by the increasingly dense coverage of thermokarst-related areas from south to north. This regionally focused procedure can be extended to other areas to provide the highly detailed periglacial terrain mapping capabilities currently lacking in global-scale permafrost datasets. |
format |
Article in Journal/Newspaper |
author |
Grosse, Guido Schirrmeister, Lutz Malthus, Timothy J |
spellingShingle |
Grosse, Guido Schirrmeister, Lutz Malthus, Timothy J Application of Landsat‐7 satellite data and a DEM for the quantification of thermokarst‐affected terrain types in the periglacial Lena–Anabar coastal lowland |
author_facet |
Grosse, Guido Schirrmeister, Lutz Malthus, Timothy J |
author_sort |
Grosse, Guido |
title |
Application of Landsat‐7 satellite data and a DEM for the quantification of thermokarst‐affected terrain types in the periglacial Lena–Anabar coastal lowland |
title_short |
Application of Landsat‐7 satellite data and a DEM for the quantification of thermokarst‐affected terrain types in the periglacial Lena–Anabar coastal lowland |
title_full |
Application of Landsat‐7 satellite data and a DEM for the quantification of thermokarst‐affected terrain types in the periglacial Lena–Anabar coastal lowland |
title_fullStr |
Application of Landsat‐7 satellite data and a DEM for the quantification of thermokarst‐affected terrain types in the periglacial Lena–Anabar coastal lowland |
title_full_unstemmed |
Application of Landsat‐7 satellite data and a DEM for the quantification of thermokarst‐affected terrain types in the periglacial Lena–Anabar coastal lowland |
title_sort |
application of landsat‐7 satellite data and a dem for the quantification of thermokarst‐affected terrain types in the periglacial lena–anabar coastal lowland |
publisher |
Norwegian Polar Institute |
publishDate |
2006 |
url |
https://epic.awi.de/id/eprint/57871/ https://epic.awi.de/id/eprint/57871/1/Grosse_2006_PolRes.pdf https://hdl.handle.net/10013/epic.841b7a1b-b37d-4f85-bcc4-17a1249096b7 |
genre |
Climate change Ice laptev Laptev Sea permafrost Polar Research Thermokarst |
genre_facet |
Climate change Ice laptev Laptev Sea permafrost Polar Research Thermokarst |
op_source |
EPIC3Polar Research, Norwegian Polar Institute, 25(1), pp. 51-67, ISSN: 0800-0395 |
op_relation |
https://epic.awi.de/id/eprint/57871/1/Grosse_2006_PolRes.pdf Grosse, G. orcid:0000-0001-5895-2141 , Schirrmeister, L. orcid:0000-0001-9455-0596 and Malthus, T. J. (2006) Application of Landsat‐7 satellite data and a DEM for the quantification of thermokarst‐affected terrain types in the periglacial Lena–Anabar coastal lowland , Polar Research, 25 (1), pp. 51-67 . doi:10.1111/j.1751-8369.2006.tb00150.x <https://doi.org/10.1111/j.1751-8369.2006.tb00150.x> , hdl:10013/epic.841b7a1b-b37d-4f85-bcc4-17a1249096b7 |
op_doi |
https://doi.org/10.1111/j.1751-8369.2006.tb00150.x |
container_title |
Polar Research |
container_volume |
25 |
container_issue |
1 |
container_start_page |
51 |
op_container_end_page |
67 |
_version_ |
1810439809791950848 |